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Transcript
1 MOVEMENT OF EARTH’S CRUST By Marvin Lowe EARTH’S CHANGING SURFACE THE FLOATING CRUST 1 First lets have a quick review of the rock cycle... 1 Let’s watch a short clip as an intro... 2 EARTH’S CHANGING SURFACE WEB LINK 2 EARTH’S CHANGING SURFACE WEB LINK 3 STRUCTURE OF THE EARTH Earth Layer Layer Radius Solid Inner Core 1300 km Liquid Outer Core 2250 km Mantle 2900 km Earth’s Crust 8 to 32 km Activity More The Four Layers The Earth is composed of four different layers. The crust is the layer that you live on, and it is the most widely studied and understood. The mantle is much hotter and has the ability to flow. The outer core and inner core are even hotter with pressures so great you would be squeezed into a ball smaller than a marble if you were able to go to the center of the Earth! The Crust The Earth's Crust is like the skin of an apple. It is very thin in comparison to the other three layers. The crust is only about 3-5 miles (8 kilometers) thick under the oceans (oceanic crust) and about 25 miles (32 kilometers) thick under the continents (continental crust). The Lithospheric Plates The crust of the Earth is broken into many pieces called plates. The plates "float" on the soft, semirigid asthenosphere. 10 10 Convection Currents The middle mantle "flows" because of convection currents. Convection currents are caused by the very hot material at the deepest part of the mantle rising, then cooling and sinking again --repeating this cycle over and over. Convection Currents The next time you heat anything like soup or water in a pan you can watch the convection currents move in the liquid. When the convection currents flow in the mantle they also move the crust. The crust gets a free ride with these currents, like the cork in this illustration. Safety Caution: Don’t get your face too close to the boiling water! 4 STRESSES In The Earth’s Crust Stresses cause deformation. Deformation - breaking, tilting, and folding of rock. Before Stress Tension Compression Shearing Activity 4 STRESSES In The Earth’s Crust Stresses cause deformation. Deformation - breaking, tilting, and folding of rock. Before Stress Tension Compression Shearing Activity There are three basic deformational forces: tensional, compressional, and transversal. Tension: are forces that pull crustal rocks apart. Compression: are forces that squeeze crustal rock together. Shearing: are forces that push crustal rock horizontally and in different directions. (Image courtesy of Michael Kimberly, North Carolina State Univ.) 5 THESE STRESSES CAN CAUSE: Bending or Folding Fracture or Faulting What is a fault? A Fault is a crack in the Earth’s crust. Where do faults occur? Most faults occur on tectonic plate boundaries. However there are some faults in the middle of plate boundaries. 6 KINDS OF FAULTS Normal Fault Thrust Fault Reverse Fault Strike Slip 8 FOLDING Fold - A bend in rock caused by stress. Anticline - An upward fold in rock. Syncline - A downward fold in rock. Folding Activity Q Type of Fault Type of Stress Normal Tension Thrust Compression Strike-Slip Shearing Image 20 Strike-Slip Faults • A type of fault where rocks on either side move past each other sideways with little up-or down motion. • Shearing causes these types of faults Normal Faults • A type of fault where the hanging wall slides downward • Tension forces cause normal faults Reverse Faults • A type of fault where the hanging wall slides up • Compression forces cause reverse faults 9 FAULT OR FOLD What four things determine if rock will fault or fold? 1. Temperature of the rock under pressure. 2. Amount of the stress applied. 3. Type of rock, fragile and brittle or ductile. 4. How was the stress applied, gradually and constantly over time or suddenly. Rapid vs. Gradual Gradual Changes: changes that happen slowly over time to change the surface of Earth Rapid changes: changes that quickly change the surface or Earth Gradual vs. Rapid Can you think of some gradual changes that change the surface of Earth? 1.Rivers... they slowly carve out rock. EXAMPLE: the grand canyon 2. Wind... sediment is slowly blown away to create different rock features EXAMPLE: huddos, arches Small changes over time add up to major changes to Earth’s surface* Gradual vs. Rapid Can you think of some things that change the Earth’s surface rapidly? 1. Earthquakes... in a matter of seconds cities can have large cracks, etc. EXAMPLE: Japan is now 10 inches closer to the US, San Andres Fault 2. Volcanoes... eruptions change the surface of Earth very quickly EXAMPLE: Mt. Saint Helens eruption, lava flows in Hawaii Earthquakes • Earthquakes are a result of motion within the earth. • This only occurs where the earth is solid and therefore can only occur within about 8 miles of the surface • Earthquakes provide the best evidence regarding the interior structure of the Earth. Earthquakes Earthquakes Earthquakes Earthquakes • An earthquake is: A sudden movement of the earth's crust caused by the release of stress accumulated along geologic faults or by volcanic activity • Earthquakes are measured using seismographs Focus is the location within the earth Focus where underground rock moves and sends out earthquake waves. Epicenter The epicenter is the location on the surface of the earth directly above the focus of an earthquake Types of WAVES... Earthquakes produce three types of waves... Primary Waves (P waves) Secondary Waves (S Waves) Surface Waves Seismic Travels Drawing Wave Through of wave Primary Solids & Liquids Wave (p wave) Secondary Only Wave Solids (s wave) Solids Surface *this wave Wave causes the most damage* Particle Motion Speed of the wave Fastest (1st to arrive) slow Combination side to side & up and down Slowest (last) 38 Volcanoes... A volcano is an opening in a planet’s surface or crust which allows hot magma, volcanic ash, and/or gasses to escape from below the surface. Volcanoes are usually found where tectonic plates are diverging (spreading apart)or subducting (one plate going under the other plate). Volcanoes... Some volcanoes are really violent and have large eruptions. Some volcanoes erupt calmly. mt. saint helens clip Europe’s biggest volcano erupts HAWAII Transfer of Energy... We have talked a little bit through out the year about the different ways energy is transfered. Do you remember so of those ways? Transfer of Energy... Do Earthquakes and Volcanoes transfer energy from Earth’s interior to the surface? How? Transfer of Energy... EARTHQUAKES... How do earthquakes transfer energy from Earth’s interior to the surface? Earthquakes create Seismic waves which transfer mechanical energy Transfer of Energy... How do Volcanoes transfer energy from Earth’s interior to the surface? Volcanoes have flowing magma or hot gasses and ash that transfer heat and mechanical energy. Different Forms of Energy In the Earth • Mechanical Energy: Energy due to motion • Heat energy: energy due to heat • Potential energy: energy that is built up but not yet released • Kinetic Energy: energy that is occurring (in motion) Modeling... • Now as a table come up with a way that you would model (show) – erosion – and – the energy buildup and release in an earthquake. – Think of ways that you could show this in a classroom 47 • ROCKS ROCK!!! 48 Types of WAVES... Types of WAVES... • Primary Waves: This is the fastest kind of seismic wave, and, consequently, the first to 'arrive' at a seismic station. The P wave can move through solid rock and fluids, like water or the liquid layers of the earth. Types of WAVES... Types of WAVES... • Secondary Waves: An S wave is slower than a P wave and can only move through solid rock, not through any liquid medium. It is this property of S waves that led seismologists to conclude that the Earth's outer core is a liquid. Types of WAVES... Types of WAVES... • Surface Waves: Travelling only through the crust, surface waves are of a lower frequency than body waves, and are easily distinguished on a seismogram as a result. Though they arrive after body waves, it is surface waves that are almost entirely responsible for the damage and destruction associated with earthquakes. This damage and the strength of the surface waves are reduced in deeper earthquakes. Candy Quakes • Materials: 1 napkin/paper towel and 1 candy bar per person (Each group member needs to have a different type of candy bar) • What to do: 1.Decide who is doing which type of stress *Each person needs to do a different type of stress* 2. 3. 4. 5. -tension -compression -shearing Get your materials Take turns performing the “stress test” Answer the questions in your bell ringer book EAT your candy bar and clean up! 52 Candy Quakes Questions… • 1. Fill out the following chart Candy Bar Stress Type Fault Type Drawing • 2. How is your candy bar similar to rock layers? 53